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971.
M. Tichomirowa H.-J. Berger E.A. Koch B.V. Belyatski J. Gtze U. Kempe L. Nasdala U. Schaltegger 《Lithos》2001,56(4):303-332
This study is an attempt to unravel the tectono-metamorphic history of high-grade metamorphic rocks in the Eastern Erzgebirge region. Metamorphism has strongly disturbed the primary petrological genetic characteristics of the rocks. We compare geological, geochemical, and petrological data, and zircon populations as well as isotope and geochronological data for the major gneiss units of the Eastern Erzgebirge; (1) coarse- to medium-grained “Inner Grey Gneiss”, (2) fine-grained “Outer Grey Gneiss”, and (3) “Red Gneiss”. The Inner and Outer Grey Gneiss units (MP–MT overprinted) have very similar geochemical and mineralogical compositions, but they contain different zircon populations. The Inner Grey Gneiss is found to be of primary igneous origin as documented by the presence of long-prismatic, oscillatory zoned zircons (540 Ma) and relics of granitic textures. Geochemical and isotope data classify the igneous precursor as a S-type granite. In contrast, Outer Grey Gneiss samples are free of long-prismatic zircons and contain zircons with signs of mechanical rounding through sedimentary transport. Geochemical data indicate greywackes as main previous precursor. The most euhedral zircons are zoned and document Neoproterozoic (ca. 575 Ma) source rocks eroded to form these greywackes. U–Pb-SHRIMP measurements revealed three further ancient sources, which zircons survived in both the Inner and Outer Grey Gneiss: Neoproterozoic (600–700 Ma), Paleoproterozoic (2100–2200 Ma), and Archaean (2700–2800 Ma). These results point to absence of Grenvillian type sources and derivation of the crust from the West African Craton. The granite magma of the Inner Grey Gneiss was probably derived through in situ melting of the Outer Grey Gneiss sedimentary protolith as indicated by geological relationships, similar geochemical composition, similar Nd model ages, and inherited zircon ages. Red Gneiss occurs as separate bodies within fine- and medium-grained grey gneisses of the gneiss–eclogite zone (HP–HT overprinted). In comparison to Grey Gneisses, the Red Gneiss clearly differs in geochemical composition by lower contents of refractory elements. Rocks contain long-prismatic zircons (480–500 Ma) with oscillatory zonation indicating an igneous precursor for Red Gneiss protoliths. Geochemical data display obvious characteristics of S-type granites derived through partial melting from deeper crustal source rocks. The obtained time marks of magmatic activity (ca. 575 Ma, ca. 540 Ma, ca. 500–480 Ma) of the Eastern Erzgebirge are compared with adjacent units of the Saxothuringian zone. In all these units, similar time marks and geochemical pattern of igneous rocks prove a similar tectono-metamorphic evolution during Neoproterozoic–Ordovician time. 相似文献
972.
Kerrie M. Swadling Herbert J. G. Dartnall John A. E. Gibson milie Saulnier-Talbot Warwick F. Vincent 《Quaternary Research》2001,55(3):380
Early Holocene sediments from a continental Antarctic lake (Ace Lake, Vestfold Hills, East Antarctica) contained abundant fossil rotifers of the genus Notholca. The fossil is similar to specimens of Notholca sp. present in modern-day Ace Lake and other fresh and brackish lakes of the Vestfold Hills. Cyanobacteria and protists (chrysophyte cysts, dinoflagellate cysts, and rhizopod tests) were also recovered from the core samples. These sediments were deposited early in the freshwater phase of Ace Lake, soon after deglaciation of the area. The occurrence of this trophically diverse assemblage of organisms at an early stage in the evolution of the lake suggests either that they were part of an endemic Antarctic flora and fauna which pre-dated the last glacial maximum and survived in glacial refugia or that efficient intercontinental dispersal had occurred. 相似文献
973.
陆相红层盆地1:5万区调中的遥感应用研究 总被引:3,自引:0,他引:3
本文采用遥感地质方法,对陆相红层盆地的沉积岩相、沉积体系界面、盆地充填序列、岩相变化以及地层格架影像特征进行了识别研究,取得了较好效果,为遥感在红层盆地1:5万区调中的应用,开辟了新思路。 相似文献
974.
作者报告了100例脑脓肿,其中一般性脑脓肿62例、脑内小脓肿38例(强化灶小于1.5cm),并对发病部位,临床表现及CT表现的主要特点进行了讨论。 相似文献
975.
本文报告了4例在妊娠期间CT检查出来脑积水畸形病例,CT表现为幕上大片低密度区域,基底节和部分枕叶地结构完整,幕上脑室系统消失,脑组织形状结构不规则,大脑镰结构完整。 相似文献
976.
孔秋雁 《CT理论与应用研究》1996,5(2):30-31
CT球管耙偏移是较为少见的,本文以GE sytec 2000i为例,详细描述了由此引起的扫描停止,机器伪影等现象及分析、处理过程,并通过与管衰老相比较。进一步述了两者的共同点及在图像质量,管电流稳定性,检测过程等方面的区别,最后总结出一套检测与判断耙心偏移的方法。 相似文献
977.
本文介绍了葛洲坝垂直位移遥控监测系统的工作原理、结构、电路设计特点及实际使用效果。几年的实测结果证明了此系统量测精度高、稳定性好、自动化程度高,实现了联机实时自动监测大坝垂直位移的目标。 相似文献
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